Excerpt from Paleontology of the Eureka District, Vol. 8
Sir: I have the honor to transmit herewith the report of Mr. Charles D. Walcott on the "Paleontology of the Eureka District"
The publication of Mr. Walcott"s monograph marks an era in the history of the Paleozoic paleontology of the Far West. Heretofore the collections of fossils obtained have been in most instances small, incomplete, and hastily gathered from more or less widely separated localities. If the species obtained proved sufficient to determine the geologic horizons for the purpose of comparative study, little more was expected.
Now we possess the results of a careful survey of a district with a rich fauna, through 30,000 feet of Paleozoic strata, representing the Cambrian, Silurian, Devonian, and Carboniferous rocks.
Mr. Walcott"s intimate knowledge of the geological and structural features of the district lends additional weight to his own special labors. I regard bis report as the most important contribution yet made to the invertebrate paleontology of the Basin Ranges, and of great value in its bearings upon the geology of the Cordillera, which under your guidance we are gradually working out.
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